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首页> 外文期刊>Limnological Review >Bottom sediments as a potential source of phosphorus in the riverine-lacustrine system of the Ko?na River (Northeastern Poland)
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Bottom sediments as a potential source of phosphorus in the riverine-lacustrine system of the Ko?na River (Northeastern Poland)

机译:底部沉积物是科纳河(波兰东北部)的河-湖泊系统中磷的潜在来源

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摘要

Sediments from hypereutrophic Lake ?ajskie localized in northeastern Poland were examined on the basis of P-fraction. The sediments were collected at five sampling sites. In the investigated lake, the rank order of P-fractions was HCl-P > BD-P > NH4Cl-P > NaOH - nrP. The loosely sorbed phosphorus NH4Cl-P represented < 3% of the sedimentary inorganic phosphorus, while the reductant phosphorus (BD-P) ranged from 2 to 10%. The calcium bound phosphorus (HCl-P) showed considerable contribution (59-74%) to the sedimentary inorganic P-loads. BDP was the most reactive fraction in Lake ?ajskie. Iron compounds and organic matter seem to play a significant role in regulating this labile P-budget.
机译:基于P-馏分,研究了位于波兰东北部的富营养化的富埃克斯基湖的沉积物。在五个采样点收集了沉积物。在所研究的湖泊中,P馏分的等级顺序为HCl-P> BD-P> NH4Cl-P> NaOH-nrP。松散吸附的磷NH4Cl-P占沉积无机磷的<3%,而还原磷(BD-P)的范围为2%至10%。钙结合的磷(HCl-P)对沉积无机P负荷表现出可观的贡献(59-74 %)。 BDP是法伊斯基湖中反应最活跃的部分。铁化合物和有机物似乎在调节这种不稳定的P预算中起着重要作用。

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